«MACRODIAGONAL»に関連する英語の本
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1
A Dictionary of Chemistry and the Allied Branches of Other ...
261, which is a form of sulphur. The brachydiagonal dome Poo truncates
symmetrically the macrodiagonal terminal edges {fig. 262), and in like manner,
the macrodiagonal dome Poo produces symmetrical truncation of the
brachydiagonal ...
2
Pamphlets on Biology: Kofoid collection
intersection of these lines, is one extremity of the macrodiagonal ; and the line E'
E, in which ME=ME', is the macrodiagonal. AA' DD', EE' are the axes in a diclinate
form in which the axes are equal. . From the observations on the preceding ...
3
American Journal of Science
The cleavage vertical prism has the angle 136° 58', which gives for the prism with
half the macrodiagonal, 103° 30', — a relation like that between hornblende and
augite. The three unit prisms, 103° 30', 58° 17', 70° 32', very nearly correspond ...
4
The American Journal of Science and Arts
They have an average length of about 0-021 mm., and a breadth of about 0-015
mm., and show, in part, the form of very sharply defined rhombic tables ; in part,
these are variously truncated on the angles connected by the macrodiagonal.
5
On hypersthene-andesite and on triclinic pyroxene in augitic ...
On determining the direction of total extinction, the (in figure) upper and lower
portions are found to agree with an angle of 27° 30' from the assumed
macrodiagonal. The central portion, however, has an angle of extinction of 10° 30
', cutting the ...
Whitman Cross, Samuel Franklin Emmons, 1884
The flake consists of three macrodiagonal lepidolite crystals, irregularly twinned
together, and the sides of the hexagon are formed principally by {010} ; {110} is
also present on one individual, and the corners of the hexagon are truncated by ...
Mineralogical Society (Great Britain), 1903
7
The Mineralogical Magazine and Journal of the Mineralogical ...
a flake from a hexagonal lepidolite prism without any central core of muscovite.
The flake consists of three macrodiagonal lepidolite crystals, irregularly twinned
together, and the sides of the hexagon are formed principally by {010} ; {110} is ...
The longer lateral axis is termed the macrodiagonal ; f and tho shorter, the
brachydiagonal.% The macropinakoids arc the faces which cut the brachy-
diagonal. while the brachypinakoids are those which cut the macrodiagonal. In
this system ...
9
A System of Mineralogy: Including an Extended Treatise on ...
If X and Z, in an inclined macrodiagonal hemiprism, are known, we have the
relation, a: c: : sin. Z sin. a : sin. X sin. y. If Y and Z, in an inclined brachydiagonal
hemiprism, are known, we may find the relative values by the proportion, a : b : :
sin.
Macrodiagonal. The longer lateral axis In the orthorhombic and trl- cllnic systems.
(Standard) Macrodome. In crystallography, a dome parallel to the macrodiagonal
(Standard) Macromeritic. Of or pertaining to a granitoid structure of rocks that Is ...
